The Greenland Ice Sheet is losing mass at an accelerating rate due to increased surface melt and flow acceleration in outlet glaciers. Quantifying future dynamic contributions to sea level requires ...
Figure 1: Last Glacial Maximum ice extent of the Eurasian ice sheet complex 8. Patches of desiccated, stiff gas-hydrate-hosting sediments and shallow bedrock beneath the Håkjerringdjupet ice stream ...
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